Lead Isotope Analysis
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Recent papers in Lead Isotope Analysis
This paper introduces the large-scale coin sampling project, Coinage and the dynamics of power: the Western Mediterranean 500-100 BC, along with the results of the archaic coins analysed. The results demonstrate that multiple silver... more
This paper introduces the large-scale coin sampling project, Coinage and the dynamics of power: the Western Mediterranean 500-100 BC, along with the results of the archaic coins analysed. The results demonstrate that multiple silver sources were accessible for minting archaic coinage, mostly consigned to the Aegean. In formulating a research design, it became apparent that long-standing and problematic issues remain with the archaeometric study of coinage (i.e. surface analyses, reference materials, data comparability). The principal purpose of this paper is to highlight the importance of a sound sampling protocol and analytical strategy for studying ancient coinage, to ensure the quality, reliability and comparability of future coin data. The paper also introduces a set of three new archaeological silver-alloy standards that can be used for studying coinage.
The conventional approach to ore provenance studies of ancient silver coins and artifacts has been to first analyze and then try to match them to published data about mining districts, a difficult task given our incomplete knowledge of... more
The conventional approach to ore provenance studies of ancient silver coins and artifacts has been to first analyze and then try to match them to published data about mining districts, a difficult task given our incomplete knowledge of these. While literary sources are useful to identify possible provenances, they potentially bias interpretations proper because of a variety of limitations of their time. Archeological evidence in the form of mining shafts, galleries, spoil heaps, and tools also provides a tangible and reliable record of mining, but dating such activity can be problematic and the record is inconsistent. Here we propose a new approach driven by Pb isotopic data rather than numismatic groups. Statistical analysis of Pb isotopic data is used to identify ore-defined isotopic clusters. This new method is based on an algorithm that predicts the number of isotopic clusters necessary to fulfill the simple condition that variance within isotopic clusters is minimized whereas inter-cluster variance is maximized. Since each cluster reflects a discrete geological episode within a particular environment broadly datable to a specific Pb model age, it can be identified as a potential source exploited by ancient miners. We explore the potential of this method in two examples using data from coins and ores respectively. In the first example, Roman Republican silver coins form three ‘end-member’ clusters sourced in mining districts with Cenozoic, Mesozoic, and Paleozoic Pb model ages. The example demonstrates how sources of silver used to mint coinage of the Roman Republic shifted within 50 years of the end of the Second Punic War in 201 BCE. In the second example using Aegean galena samples, Pb isotopes distinguish components with model ages datable to the Hercynian basement, the recent Aegean tectonic province, and Cyprus, noting that significant silver mining districts may remain unidentified in either Spain or the Aegean world. We further clarify a number of potential analytical issues and advocate that users of Pb isotopes for tracing archeological artifacts measure all four lead isotopes and inspect the 12 proposed isotope combinations in order to select those that provide the best rep-resentation of the data. We also emphasize that full advantage should be taken of the geologically informed parameters (model age and Th/U/Pb relationships) to identify the geological context of metal sources.
The aim of this article is to reinterpret a well-known underwater archaeological site located at Las Amoladeras, in La Manga del Mar Menor, near Cabo de Palos. For this purpose, after a historiographical review of the existing... more
The aim of this article is to reinterpret a well-known underwater archaeological site located at Las Amoladeras, in La Manga del Mar Menor, near Cabo de Palos. For this purpose, after a historiographical review of the existing bibliography, we have studied, contextualized and undertaken isotopic analyses of some of the most interesting material from this archaeological site, as well as a plomo monetiforme (coin-like lead token) of the same type as those recovered at Las Amoladeras and the ones that circulated in the Balearic Islands. The lead isotope analyses carried out on the aforementioned artefacts allow us to determine the origin of the ore used in the first two objects as Cartagena – Mazarrón and the Sierra Morena respectively. However, the lead used in the manufacture of the plomo monetiforme seems to reflect a mixture of metals. Based on all the above, we interpret this site as the remains of a shipwreck dating from the 50-30 B.C. that was carrying a cargo composed in part, if not almost exclusively, of metallic items, mostly lead objects, probably to be sold and recycled. Las Amoladeras can therefore be contextualized in a very specific historical and economic framework, that of the commercialization and reuse of the lead in late Republican Hispania.
A previous analysis of Omaha skeletons dating between A.D. 1780 and 1820 revealed the presence of lead in all skeletons with high concentrations in children and adult males (Reinhard and Ghazi [1992] Am. J. Phys. Anthropol. 89: 183-195).... more
A previous analysis of Omaha skeletons dating between A.D. 1780 and 1820 revealed the presence of lead in all skeletons with high concentrations in children and adult males (Reinhard and Ghazi [1992] Am. J. Phys. Anthropol. 89: 183-195). Two likely explanations for the high lead levels were presented: 1) metabolic absorption of lead and 2) diagenetic uptake of lead by the bones from postmortem application of pigments to the corpse. Two types of lead were available to the Omaha tribe: 1) Mississippi Valley type, and 2) non-Mississippi Valley type. It has been suggested that red-lead pigment mixed with mercury sulfide (cinnabar) applied to the corpse may have been one of the sources of lead found in bones. Further isotopic analyses of samples of pigment and metallic lead artifacts associated with the skeletons revealed that non-Mississippi Valley type lead is present in the pigment while Mississippi Valley type lead comes from metallic artifacts. Both lead and mercury were found in the pigment samples, verifying that a lead-based pigment mixed with cinnabar-based pigment was used as a cosmetic by the Omaha. Isotopic analysis of lead in skeletons indicates that the pigment contributed most to lead content of bone. This new evidence clarifies the previous study and suggests specific mechanisms by which lead became incorporated into bone.
The Celò hoard (half XII-beginning XI century BC), along with other contemporary bronzes from the Natisone Valleys, is meaningful to understand the role of this river route during the Late Bronze Age. In a century, the Natisone Valleys... more
The Celò hoard (half XII-beginning XI century BC), along with other contemporary bronzes from the Natisone Valleys, is meaningful to understand the role of this river route during the Late Bronze Age. In a century, the Natisone Valleys see the increasing importance of their mediating role, which is emphasized by the strategic position in the middle of the routes connecting the alpine and transalpine mining regions with the Padano-Veneto sites and the Danube- Balkan districts. Initially (BM-BR1), they were involved in widespread exchanges and represented one of the many trade routes of the period. In the following phase (BR2-BF1), they are in the process of becoming preferential interlocutors up to mediate systematic and exclusive relationships between these areas at the later stage (BF2). Due to their proximity both to the alpine mining sites and the Friulian plain, the Natisone Valleys represented important crossing points for metal supply. Most of the Celò bronzes belongs to alpine typologies and this may mean that these regions are preferred for relationships. This evidence would even be strengthened by the archaeometric analysis: the copper of some bronzes would have a south-alpine origin (Trentino Alto-Adige and Veneto), instead of that of others would have a transalpine origin (Austria and Switzerland), but, as regards the latter, there are still some doubts.
This interdisciplinary project aims to contribute to elucidate the integral role of trade and supply in Rome’s global empire by employing techniques associated with archaeometry to the study of ceramic and lead objects. By documenting and... more
This interdisciplinary project aims to contribute to elucidate the integral role of trade and supply in Rome’s global empire by employing techniques associated with archaeometry to the study of ceramic and lead objects.
By documenting and quantifying new archaeological evidence for contacts, commercial circuits and trade networks between the principal confederations of southern Gaul (France), Hispania Citerior (Spain), and the peoples of the Italian peninsula during the late Roman Republic and the transition into the Empire (2nd-1st c. B.C.E.), the project explores the extent to which this ancient global market created asymmetrical socio-economic relationships of domination and exploitation between and within production and consumption centers.
By documenting and quantifying new archaeological evidence for contacts, commercial circuits and trade networks between the principal confederations of southern Gaul (France), Hispania Citerior (Spain), and the peoples of the Italian peninsula during the late Roman Republic and the transition into the Empire (2nd-1st c. B.C.E.), the project explores the extent to which this ancient global market created asymmetrical socio-economic relationships of domination and exploitation between and within production and consumption centers.
The geochemical analysis of oxhide ingots from Eastern Bulgarian museums is a compulsory step towards a convincing explanation of these objects. Being the hallmark of Late Bronze Age trade in the eastern Mediterranean, oxhide ingots are... more
The geochemical analysis of oxhide ingots from Eastern Bulgarian museums is a compulsory step towards a convincing explanation of these objects. Being the hallmark of Late Bronze Age trade in the eastern Mediterranean, oxhide ingots are among the few commodities passing over the economic and cultural confines of the Aegean into continental
Europe. Their presence on the continent seems enigmatic, because written and archaeological sources bear no record on Eastern Mediterranean interest for the north.
It is not proposed to offer a general interpretation of all oxhide ingots in non-Mediterranean contexts. The main goal is to shed light on the factors which contributed to the appearance of these foreign objects in the Lower Danube region and the lands to the south of the Stara
Planina Mountains. The situation is somewhat similar to clearly Cypriot oxhide ingots in Sardinia, and we will explore the possibility that in the case of the eastern Balkans it was not a Mediterranean trading network but a local initiative. The hoard from Kozman Dere (Şarköy, Tekirdağ in Turkey), which is a peculiar collection demonstrating an amazing mixture of Mediterranean and Balkan type metal objects (including a fragment of an oxhide ingot), may indicate that the region of the Dardanelles could have been a gateway hub. Whether this transition meant the loss of all
‘Mediterranean values and connotations’ of the oxhide ingots, or whether some of these accompanied the objects and were incorporated in eastern Balkan social practices is extremely difficult to decide due to the largely unknown find contexts and thus difficult dating evidence.
Europe. Their presence on the continent seems enigmatic, because written and archaeological sources bear no record on Eastern Mediterranean interest for the north.
It is not proposed to offer a general interpretation of all oxhide ingots in non-Mediterranean contexts. The main goal is to shed light on the factors which contributed to the appearance of these foreign objects in the Lower Danube region and the lands to the south of the Stara
Planina Mountains. The situation is somewhat similar to clearly Cypriot oxhide ingots in Sardinia, and we will explore the possibility that in the case of the eastern Balkans it was not a Mediterranean trading network but a local initiative. The hoard from Kozman Dere (Şarköy, Tekirdağ in Turkey), which is a peculiar collection demonstrating an amazing mixture of Mediterranean and Balkan type metal objects (including a fragment of an oxhide ingot), may indicate that the region of the Dardanelles could have been a gateway hub. Whether this transition meant the loss of all
‘Mediterranean values and connotations’ of the oxhide ingots, or whether some of these accompanied the objects and were incorporated in eastern Balkan social practices is extremely difficult to decide due to the largely unknown find contexts and thus difficult dating evidence.
The first half of this article is a brief critical history of the use of lead isotopes for inferring the geological provenance of archaeological materials, with emphasis on non‐ferrous metals. The second half examines variation in the... more
The first half of this article is a brief critical history of the use of lead isotopes for inferring the geological provenance of archaeological materials, with emphasis on non‐ferrous metals. The second half examines variation in the lead isotopic ratios of oxide and sulphide ore minerals in selected regions of the world, and relates these to the geological histories of ore formation in each region. This exercise shows that in regions where most ore deposits are of similar geological age ‐ as in the Andes, Europe, and the circum‐Mediterranean ‐ provenance analysis with lead isotopes is inherently difficult because geographically distant sources often exhibit similar isotopic ratios. Conversely, regions with many periods of ore formation – like southern Africa – appear to be very promising regions for future studies of provenance with lead isotopes. The wider implication of our exploratory survey is that archaeologists should consider carefully the range and clustering of geological lead isotopic ratios in their regions of interest before investing large sums of money in lead isotopic analysis of artefacts.
Copper was highly valued in sub-Saharan Africa for jewellery and as a store of wealth, but was rarely used for tools or weapons. The Central African Copperbelt is one of the world's largest copper deposits, and is known to have been mined... more
Copper was highly valued in sub-Saharan Africa for jewellery and as a store of wealth, but was rarely used for tools or weapons. The Central African Copperbelt is one of the world's largest copper deposits, and is known to have been mined since at least 400–600 cal CE, but has seen very little archaeological investigation. We measured lead isotope ratios and trace element concentrations in 20 copper objects, dating between ca. 650 cal CE and ca. 1200 cal CE, from two sites in the Tsodilo Hills in northwestern Botswana. The results show unequivocally that almost all derive from Copperbelt ore deposits in Katanga Province, Democratic Republic of the Congo, at least 1050 km from Tsodilo. Our results are very similar to those recently obtained for a suite of 45 copper ingots, dated between 9th and 18th centuries cal CE, most of which are from cemeteries in the Upemba Depression, about 200 km north of the Copperbelt (Rademakers et al., 2019).
Because of the fact that pigments are not ubiquitous in the archeological record, the application of noninvasive analytical methods is a necessity. In this work, pink and purple lake pigments recovered from the excavations of the ancient... more
Because of the fact that pigments are not ubiquitous in the archeological record, the application of noninvasive analytical methods is a necessity. In this work, pink and purple lake pigments recovered from the excavations of the ancient city of Pompeii (Campania, Italy) and preserved in their original bowls at the Naples National Archaeological Museum (Italy) were analyzed to characterize the composition of their inorganic binders (mordants). In situ preliminary analyses using a hand held energy dispersive X-ray fluorescence spectrometer (HH-ED-XRF) allowed us to determine the use of an aluminosilicate enriched in Cu and Pb. Scanning electron microscopy coupled to energy dispersive X-ray spectrometry (SEM-EDS) and benchtop ED-XRF analyses confirmed these results, while inductively coupled plasma mass spectrometry (ICPMS) allowed one to determine the concentration of major, minor, and trace elements. The use of other techniques such as X-ray diffraction (XRD), and micro-Raman and infrared spectroscopies allowed one to characterize the pigments at the molecular level. The high concentration of Cu detected in the pigments (1228−12937 μg g−1) could be related to the addition of Cu salts to obtain the desired final hue. The concentrations of Pb (987−2083 μg g−1) was also remarkable. Lead isotopic ratio analysis (206Pb/207Pb) suggested a possible origin related to the leaching of the ancient lead pipes from Pompeii and the subsequent transfer to the buried pigments or to the inorganic binder. Molecular analysis also showed that the binder is composed of an allophane-like clay. Moreover, it was possible to determine that to obtain the final purple hue of a specific pigment, Pompeian blue pigment was also mixed into the dyed clay.
Following animated discussions in the 1990–2010 period concerning the validity and potential application of Pb isotope data to yield information on ancient metallurgy, recently lead isotope analysis has been extensively applied with... more
Following animated discussions in the 1990–2010 period concerning the validity and potential application of Pb isotope data to yield information on ancient metallurgy, recently lead isotope analysis has been extensively applied with alternate success and difficulty to the early stages of copper/lead/silver/tin metal flow in the Central Mediterranean area, arbitrarily defined as including Italy, the Mediterranean Islands, and the surrounding regions for comparison purposes. A wealth of data are now available in the literature, many of them interpreted within local contexts and limited geographical extension, and often within a shifting conceptual modeling frame. A brief review of the recently published data indicate that the metal flow in prehistory and protohistory is far more dynamic than presumed on the basis of the traditionally assumed archaeological models. It is suggested that the isotopic tracers, if correctly applied and interpreted, may substantially help in decoding the metal exploitation and trade patterns at different scales, from the local links between mines and smelting sites to wider regional or long‐distance trades. The abundant dataset available are however in need of thorough interpretation in terms of wider archaeological and archaeo‐metallurgical questions, possibly by the use of advanced statistical methods and unconventional data mining protocols.
Atmospheric metal pollution is a major health concern whose roots pre-date industrialization. This study pertains the analyses of ancient human skeletons and compares them with natural archives to trace historical environmental exposure... more
Atmospheric metal pollution is a major health concern whose roots pre-date industrialization. This study pertains the analyses of ancient human skeletons and compares them with natural archives to trace historical environmental exposure at the edge of the Roman Empire in NW Iberia. The novelty of our approach relies on the combination of mercury, lead and lead isotopes. We found over a 700-year period that rural Romans incorporated two times more mercury and lead into their bones than post-Romans inhabiting the same site, independent of sex or age. Atmospheric pollution sources contributed on average 57% (peaking at 85%) of the total lead incorporated into the bones in Roman times, which decreased to 24% after the decline of Rome. These values and accompanying changes in lead isotopic composition mirror changes in atmospheric Pb deposition recorded in local peatlands. Thus, skeletons are a time-transgressive archive reflecting contaminant exposure.
Two large complexes of struck lead pieces, from the Roman colony of Minturnae and from Baetica (southern Spain) in the late Republic, have been documented in recent years. There are close and unique iconographic parallels between them. We... more
Two large complexes of struck lead pieces, from the Roman colony of Minturnae and from Baetica (southern Spain) in the late Republic, have been documented in recent years. There are close and unique iconographic parallels between them. We accordingly undertook an analysis of the isotopic signatures of the leads used in the two areas, to see if this aids in understanding their relationship. At the same time, we investigated the presence of tin in the alloys of both complexes, and its implications. The two complexes both largely used lead from the massively productive Cartagena-Marrazón area, but that each also had another separate supply. We then expanded to a consideration of the evidence of the presence in Carthago Nova of Italian gentes known from the area of Minturnae in the second and first centuries, and their role in the production of, and trade in, Spanish lead. This allowed us to identify a die-linked series among the lead pieces from Minturnae, signed by members of some of the most prominent gentes at Carthago Nova, which we suggest is evidence of a company (societas) trading between the two ports. We also investigated possible contacts with Minturnae of the gentes signing the Baetican complex. We conclude that the central role of Minturnae as a Republican port trading with Spain has been under-estimated, and that it played a key role in the early colonisation and exploitation of Hispania.
Open access; free download from https://doi.org/10.1371/journal.pone.0227259 The paper discusses results of an interdisciplinary research project integrating lead isotope, chemical, and archaeological analysis of 20 early metal objects... more
Open access; free download from https://doi.org/10.1371/journal.pone.0227259
The paper discusses results of an interdisciplinary research project integrating lead isotope, chemical, and archaeological analysis of 20 early metal objects from central Italy. The aim of the research was to develop robust provenance hypotheses for 4th and 3rd millennia BC metals from an important, yet hitherto neglected, metallurgical district in prehistoric Europe, displaying precocious copper mining and smelting, as well as socially significant uses of metals in ‘Rinaldone-style’ burials. All major (and most minor) ore bodies from Tuscany and neighbouring regions were characterised chemically and isotopically, and 20 Copper Age axe-heads, daggers and halberds were sampled and analysed. The objects were also reassessed archaeologically, paying special attention to find context, typology, and chronology. This multi-pronged approach has allowed us to challenge received wisdom concerning the local character of early metal production and exchange in the region. The research has shown that most objects were likely manufactured in west-central Italy using copper from Southern Tuscany and, quite possibly, the Apuanian Alps. A few objects, however, display isotopic and chemical signatures compatible with the Western Alpine and, in one case, French ore deposits. This shows that the Copper Age communities of west-central Italy participated in superregional exchange networks tying together the middle/upper Tyrrhenian region, the western Alps, and perhaps the French Midi. These networks were largely independent from other metal displacement circuits in operation at the time, which embraced the north-Alpine region and the south-eastern Alps, respectively.
The paper discusses results of an interdisciplinary research project integrating lead isotope, chemical, and archaeological analysis of 20 early metal objects from central Italy. The aim of the research was to develop robust provenance hypotheses for 4th and 3rd millennia BC metals from an important, yet hitherto neglected, metallurgical district in prehistoric Europe, displaying precocious copper mining and smelting, as well as socially significant uses of metals in ‘Rinaldone-style’ burials. All major (and most minor) ore bodies from Tuscany and neighbouring regions were characterised chemically and isotopically, and 20 Copper Age axe-heads, daggers and halberds were sampled and analysed. The objects were also reassessed archaeologically, paying special attention to find context, typology, and chronology. This multi-pronged approach has allowed us to challenge received wisdom concerning the local character of early metal production and exchange in the region. The research has shown that most objects were likely manufactured in west-central Italy using copper from Southern Tuscany and, quite possibly, the Apuanian Alps. A few objects, however, display isotopic and chemical signatures compatible with the Western Alpine and, in one case, French ore deposits. This shows that the Copper Age communities of west-central Italy participated in superregional exchange networks tying together the middle/upper Tyrrhenian region, the western Alps, and perhaps the French Midi. These networks were largely independent from other metal displacement circuits in operation at the time, which embraced the north-Alpine region and the south-eastern Alps, respectively.
Objectives: A multi-isotope study was conducted on individuals buried at Skriðuklaustur monastery (AD 1493–1554) to investigate their geographic origins and dietary composition. Comparative material from individuals excavated from... more
Objectives: A multi-isotope study was conducted on individuals buried at
Skriðuklaustur monastery (AD 1493–1554) to investigate their geographic origins and dietary composition. Comparative material from individuals excavated from Skeljastaðir, an inland farm site was also analyzed.
Materials and methods: Bone collagen was extracted from 50 humans
(Skriðuklaustur and Skeljastaðir) and 25 animals (Skriðuklaustur) and analyzed for δ13C, δ15N, and δ34S. Dental enamel samples from 31 individuals (Skriðuklaustur) were also analyzed for 87Sr/86Sr, δ18O, δ13C, and trace elements (Pb, Sr, Zn, Ba).
Results: The mean value determined from individuals from Skriðuklaustur (n = 36) was δ13C = −18.7 ± 0.8‰, δ15N = 12.8 ± 1.1‰, and δ34S = 9.0 ± 1.6‰, whereas at Skeljastaðir (n = 14), it was δ13C = −20.5 ± 0.8‰, δ15N = 7.8 ± 0.9‰, and δ34S = 9.4 ± 1.6‰. At Skriðuklaustur, human dental enamel samples (n = 31) provided a 87Sr/86Sr range of 0.7060–0.7088, δ18Ophosphate from 13.9 to 16.1‰ and δ13Ccarbonate from −16.6 to −12.9‰. Inferred drinking water (δ18Odw) values range from −12.3 to −8.9‰. Sr concentrations range from 25.8 to 156.7 ppm, Ba from 0.11 to 0.81 ppm, Zn from 43.8 to 145.8 ppm, and Pb from 0.13 to 9.40 ppm.
Discussion: A combination of results indicates that the people from Skriðuklaustur were born in Iceland, but some lived inland during childhood while others lived closer to the coast. Since Skriðuklaustur was a hospital, these individuals may have sought medical treatment at the monastery. The δ13C and δ15N values determined from bone collagen indicate that the people residing at Skriðuklaustur consumed a diet high in marine protein, while those residing at Skeljastaðir exhibit values more consistent with terrestrial resources.
Skriðuklaustur monastery (AD 1493–1554) to investigate their geographic origins and dietary composition. Comparative material from individuals excavated from Skeljastaðir, an inland farm site was also analyzed.
Materials and methods: Bone collagen was extracted from 50 humans
(Skriðuklaustur and Skeljastaðir) and 25 animals (Skriðuklaustur) and analyzed for δ13C, δ15N, and δ34S. Dental enamel samples from 31 individuals (Skriðuklaustur) were also analyzed for 87Sr/86Sr, δ18O, δ13C, and trace elements (Pb, Sr, Zn, Ba).
Results: The mean value determined from individuals from Skriðuklaustur (n = 36) was δ13C = −18.7 ± 0.8‰, δ15N = 12.8 ± 1.1‰, and δ34S = 9.0 ± 1.6‰, whereas at Skeljastaðir (n = 14), it was δ13C = −20.5 ± 0.8‰, δ15N = 7.8 ± 0.9‰, and δ34S = 9.4 ± 1.6‰. At Skriðuklaustur, human dental enamel samples (n = 31) provided a 87Sr/86Sr range of 0.7060–0.7088, δ18Ophosphate from 13.9 to 16.1‰ and δ13Ccarbonate from −16.6 to −12.9‰. Inferred drinking water (δ18Odw) values range from −12.3 to −8.9‰. Sr concentrations range from 25.8 to 156.7 ppm, Ba from 0.11 to 0.81 ppm, Zn from 43.8 to 145.8 ppm, and Pb from 0.13 to 9.40 ppm.
Discussion: A combination of results indicates that the people from Skriðuklaustur were born in Iceland, but some lived inland during childhood while others lived closer to the coast. Since Skriðuklaustur was a hospital, these individuals may have sought medical treatment at the monastery. The δ13C and δ15N values determined from bone collagen indicate that the people residing at Skriðuklaustur consumed a diet high in marine protein, while those residing at Skeljastaðir exhibit values more consistent with terrestrial resources.
Resumen: En este trabajo se examinan los resultados de varias series analíticas de minerales y objetos arqueo-lógicos procedentes de las Islas Baleares. En total, se presentan análisis de composición elemental y de isótopos de plomo de 13... more
Resumen: En este trabajo se examinan los resultados de varias series analíticas de minerales y objetos arqueo-lógicos procedentes de las Islas Baleares. En total, se presentan análisis de composición elemental y de isótopos de plomo de 13 muestras de galenas de depósitos de Mallorca y Menorca, así como de 18 objetos arqueológicos elaborados en plomo y en aleaciones ternarias ricas en este metal, todos procedentes de distintas necrópolis mallorquinas de cronología postalayótica (c. 550-123 a. C.). El objetivo del estudio es analizar la circulación del plomo y obtener información sobre las estrategias de gestión y consumo de este metal por parte de las comuni-dades locales durante la Segunda Edad del Hierro. Los datos aportados permiten realizar análisis comparativos que, junto a los ya existentes generados por otros proyectos, proporcionan una perspectiva más definida sobre la integración de las Islas Baleares en el panorama de los circuitos de intercambio mediterráneos durante estas cronologías. Los resultados también reflejan la complejidad de dichas redes, en las que el mundo fenicio-púnico tiene un papel especialmente relevante, aunque, paralelamente, se intuye el aprovechamiento de recursos locales por parte de las comunidades indígenas del archipiélago. Palabras clave: arqueometalurgia; análisis de isótopos de plomo; postalayótico; mundo fenicio-púnico; Me-diterráneo; Mallorca; minerales de plomo. Abstract: This paper examines the results of a series of analyses of minerals and archaeological objects from the Balearic Islands. In total, it presents the analytical results of the elemental and lead isotope compositions of 13 samples of galena deposits from Mallorca and Minorca, in addition to 18 archaeological objects made of lead and lead-rich ternary alloys from different Mallorcan necropolises from the Post-Talayotic period (c. 550-123 bc). The aim of the study is to analyse the circulation of lead and to gain an insight into strategies for the management and consumption of this metal by local communities during the Late Iron Age. With these data, comparative analyses can be made and, combined with data from other projects, a better vision can be gained on the Balearic Islands' integration in Mediterranean trade routes during this period. The results also reflect the complexity of these networks, in which the Punic-Phoenician world played a particularly important role, although, in parallel with this, the use of local resources by local native Balearic communities can be inferred.
The proposed project deals with advanced archaeometric studies of specialised production and distribution patterns from the 4th century BC to the 1st century AD. Changing patterns in acquisition and properties of source materials indicate... more
The proposed project deals with advanced archaeometric studies of specialised production and distribution patterns from the 4th century BC to the 1st century AD. Changing patterns in acquisition and properties of source materials indicate shifts in resources, technology, organisational process, custom demands, or more profound socio-cultural phenomena. Exact data on trends in using materials in prehistory creates a solid part of the archaeological narration and their importance – as an exact base for interpretation - is indisputable. In this project we focus on copper-alloys, precious metals, and glass. Artefacts made of these materials stand out as important markers of identity, mobility, status and economic strategies. Based on diachronic case studies on their sourcing, production, and distribution and by application of the trace element and isotopic analyses we aim to discover or verify major trends in socio-economic development in one of the most dynamic periods in prehistory.
Recently we have started to relate the mobility of objects to mobility of people, applying the analyses of the isotopes of Sr and Pb to La Tene graves from the 4th to 2nd centuries BC.
Aims:
By archaeometry of non-ferrous metals and glass we aim to reveal trends in socio-economic development of the La Tène and Early Roman period: sourcing of materials, spread of innovations, mobility, distribution patterns, life cycles and the question of so called production crisis in the 1st cent. BC.
Recently we have started to relate the mobility of objects to mobility of people, applying the analyses of the isotopes of Sr and Pb to La Tene graves from the 4th to 2nd centuries BC.
Aims:
By archaeometry of non-ferrous metals and glass we aim to reveal trends in socio-economic development of the La Tène and Early Roman period: sourcing of materials, spread of innovations, mobility, distribution patterns, life cycles and the question of so called production crisis in the 1st cent. BC.
This paper discusses a rod tripod found in tomb 64 in the area Quagliotti in Sirolo (Ancona), a sector of a necropolis of the ancient Picenean settlement of Numana. In the first part of the paper the burial context and its assemblage are... more
This paper discusses a rod tripod found in tomb 64 in the area Quagliotti in Sirolo (Ancona), a sector of a necropolis of the ancient Picenean settlement of Numana. In the first part of the paper the burial context and its assemblage are briefly introduced, with some remarks on the structure of the grave and on the spatial distribution of the objects inside the chamber. The tripod is then analysed in detail: according to the few comparisons available, it can be attributed to a type of rod tripods that were probably manufactured in Urartu during the 8th century BC. The results of lead isotope analysis attached to the paper do not invalidate this attribution. The considerable chronological hiatus between the tripod and the rest of the grave assemblage, which dates to the end of the 5th century BC, allows some considerations regarding the ancient route that brought the tripod to Numana and its possible status as a “curated” object.
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